 REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY  | REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
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REAL TIME THERMAL IR IMAGERY (UPDATED EVERY 30 MINUTES) | 
REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES) |
 REAL TIME WIND AND IR IMAGERY |  REAL TIME DVORAK TIME SERIES |
 WUNDERGROUND REAL TIME IMAGERY |  REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE) |
 FORECAST TRACK |  TRACK, RAINFALL AND CURRENT INTENSITY (UPDATED EVERY 6 HRS) |
 RELATIVE VORTICITY |  WIND SHEAR |
 VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY) |  VISIBLE MODIS IMAGERY (250M ZOOOM) |
 SATCON AMSU BRIGHTNESS TEMPERATURE |  SATCON WIND CHART |
 LOW LEVEL CONVERGENCE (CLICK TO VIEW LARGER): To identify potential areas where TC development may occur. Since the development of the TC secondary circulation (low-level inflow, updrafts in the TC eyewall, and upper-level outflow) is essential in the maturation and sustainment of a TC, identification of regions where strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments |  UPPER LEVEL DIVERGENCE (CLICK TO VIEW LARGER): To estimate the strength of the TC secondary circulation, including the low-level inflow into the TC core, the convective updraft strength within the TC eyewall, and the resulting outflow/venting at the top of the TC. This dynamic can be important for storm growth and development |
 SHALLOW LAYER STEERING |  MIDDLE LAYER STEERING |  DEEP LAYER STEERING |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS
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